Ovens Anticline #3

Detailed view of central part of the [beach section](https://sketchfab.com/3d-models/ovens-anticline-beach-section-bd35dca9e057420b812d068afb5d635c) which is parallel to a northeast-trending anticline. The rocks are interbedded slate and metasandstone of the Cambrian-Ordovician turbidite package of the Meguma Supergroup. The nested bedding-parallel quartz veins prominently display the geometry and exposure length of the fold hinge. The veins tend to thicken in the hinge and others are folded. There are cross-cutting faults on the immediate limbs, some of which might be interpreted as part of hinge thrusts. Approximately 220 images taken with a Phantom 4 Pro. West of the Ovens Park near Lunenburg, Nova Scotia Canada. (44.31573 N, 64.26887 W)